Download Download

Total Page:16

File Type:pdf, Size:1020Kb

Download Download Rivista Italiana di Paleontologia e Stratigrafia (Research in Paleontology and Stratigraphy) vol. 125(3): 587-608. November 2019 RECENT BRACHIOPODS FROM THE TONGA ISLANDS, SW PACIFIC: TAXONOMY AND BIOGEOGRAPHY MARIA ALEKSANDRA BITNER Institute of Paleobiology, Polish Academy of Sciences, ul. Twarda 51/55, 00-818 Warszawa, Poland. E-mail: [email protected] To cite this article: Bitner M.A. (2019) - Recent brachiopods from the Tonga Islands, SW Pacific: taxonomy and biogeography. Riv. It. Paleont. Strat., 125(3): 587-608. Keywords: Brachiopoda; systematics; biodiversity; Pacific archipelagos; BORDAU 2. Abstract. Twenty species of Recent brachiopods belonging to the genera Neoancistrocrania, Basiliola, Basiliolella, Dyscolia, Abyssothyris, Xenobrochus, Terebratulina, Fallax, Septicollarina, Frenulina, Amphithyris, Annuloplatidia, Leptothyrella, Dallina, Campages, Thecidellina and Minutella have been identified in the material collected during the French cruise BORDAU 2 to the Tonga Islands, South-West Pacific. Apart from Frenulina sanguinolenta all species represent the first records for the Tonga Islands. The investigated brachiopod fauna shows the greatest affinity to that from Fiji and New Caledonia, having 16 and 12 species in common, respectively. Although less affinity is observed with the New Zealand fauna, there are two species, Terebratulina australis and Amphithyris buckmani reported so far only from New Zealand, Fiji and Tonga. The biodiversity of brachiopods in Tonga is similar to that in Fiji but half as great as that in New Caledonia and New Zealand regions and much higher than in French Polynesia. INTRODUCTION origin, the eastern non-volcanic coral limestone. So far only two species, Novocrania turbinata (Poli, 1795) Since 1976 the South-West Pacific region has and Frenulina sanguinolenta (Gmelin, 1791) have been been intensively surveyed within the program Trop- reported from Tonga (Saito & Endo 2001; Logan ical Deep-Sea Benthos (formerly MUSORSTOM) 2007; Robinson 2017). Although both species are established by the Muséum national d’Histoire na- well known and widely distributed in the western turelle (Paris, France) and the Institut de Recher- Pacific, in the studied material they are either absent che pour le Développement (Nouméa, New Cale- (N. turbinata), or very rare (F. sanguinolenta). How- donia). The present report focuses on the Tonga ever, Robinson (2017) recognized N. turbinata in the island group, explored during the cruise BORDAU 2 University of Tokyo collection from Tonga. Among in 2000. The name of the cruise refers to the BOR- the 20 species identified in the studied material, 19 Der of the Indo-AUstralian plate (Bouchet et al. are reported for the first time from the Tonga Is- 2008). Tonga, comprising more than 170 islands, lands. is an archipelago in the South Pacific Ocean close to Fiji, about two-thirds of the way from Hawaii to New Zealand (Fig. 1). It lies along the boundary of the Pacific and Indian-Australian tectonic plates MATERIAL AND METHODS and consists of two geologically different, parallel The material presented here was collected during the cruise chains of islands; the western islands are of volcanic Bordau 2 (https://expeditions.mnhn.fr/campaign/bordau2) to the Tonga Islands, SW Pacific (Fig. 1). The expedition was organized by the Muséum national d’Histoire naturelle, Paris and by the Institut Received: March 12, 2019; accepted: May 17, 2019 de la Recherche pour le Développement, Nouméa, New Caledonia 588 Bitner M.A. Class CRANIATA Williams, Carlson, Brunton, Holmer & Popov, 1996 Order Craniida Waagen, 1885 Superfamily Cranioidea Menke, 1828 Family Craniidae Menke, 1828 Genus Neoancistrocrania Laurin, 1992 Type species - Neoancistrocrania norfolki Laurin, 1992, by original designation of Laurin (1992: 344) Neoancistrocrania norfolki Laurin, 1992 Fig. 2A-C 1992 Neoancistrocrania norfolki Laurin, pp. 344-346, pl. 1, figs. 1-6, pl. 2, figs. 1-6. 1997 Neoancistrocrania norfolki - Laurin, pp. 417-418, fig. 41A-E. 2009 Neoancistrocrania norfolki - Bitner, p. 6, fig. 2A-F. 2010 Neoancistrocrania norfolki - Zezina, p. 1179. 2014a Neoancistrocrania norfolki - Robinson, fig. 3A-H. 2014b Neoancistrocrania norfolki - Robinson, p. 542, fig. 2A-E. 2015 Neoancistrocrania norfolki - Bitner, p. 35, fig. 2A-B. Material examined: Tonga, BORDAU 2 cruise, stn DW 1535, one dorsal valve (MNHN IB-2013-678); stn DW 1602, one dorsal valve (MNHN IB-2013-679); stn DW 1605, one ventral valve, broken (MNHN IB-2013-680). Depth range: 263-441 m. Measurements: Max. length 14.8 mm, width 20.8 mm. Remarks. Neoancistrocrania norfolki is very rare in the studied material, found in only 3 stations. Morphologically this species is readily distinguished Fig. 1 - Map of Tonga Islands, showing location of the brachio- from Novocrania Lee & Brunton, 2001 by its massive, pod-bearing stations. mineralized ventral valve and two erect divergent processes on the dorsal valve interior (Laurin 1992, on R.V. “Alis” and carried out from 31 May 2000 to 22 June 2000. 1997; Bitner 2009, 2015) and by unique features of Brachiopods were found in 69 out of 138 stations. The exact loca- tion, depth and species identified at each stations are given in the the soft tissues (Robinson 2014a, 2014b). However, Appendix. Although the collection is rich overall (1212 specimens), molecular analysis shows that “Neoancistrocrania is nine species are rare (3 or fewer specimens). no more distantly related to the Northern clade of Samples were collected using a Warén dredge (DW) or a Novocrania than are other Novocrania clades” (Cohen trawl (CP, CH). To remove soft tissues, specimens were treated with hypochlorite bleach, followed by a water wash. For scanning elec- et al. 2014: 145) suggesting generic synonymy of tron microscope (SEM) examination, the selected specimens were Neoancistrocrania under Novocrania. Such conflict be- mounted on stubs, coated with platinum, and investigated using a tween the morpho-classification and molecular sys- Philips XL-20 microscope at the SEM laboratory of the Institute of tematics is observed in other brachiopod groups as Paleobiology, Warszawa. All the material is deposited in the collection of the Museum national d’Histoire naturelle, Paris, France under the well (Cohen & Bitner 2013; Bitner & Cohen 2015). catalogue number MNHN IB-2009-516 to IB-2009-562, IB-2009- Previously N. norfolki had been found only in 1198, IB-2009-1240, IB-2013-678 to IB-2013-790. the West Pacific (Laurin 1997; Bitner 2009, 2015; Cohen et al. 2008, 2014). The present finding ex- tends its geographical range eastward. SYSTEMATIC PART Subphylum RHYNCHONELLIFORMEA Phylum BRACHIOPODA Duméril, 1805 Williams, Carlson, Brunton, Holmer & Popov, 1996 Subphylum CRANIIFORMEA Popov, Bassett, Class RHYNCHONELLATA Williams, Carlson, Holmer & Laurie, 1993 Brunton, Holmer & Popov, 1996 Recent brachiopods from the Tonga Islands, SW Pacific 589 Fig. 2 - A-C - Neoancistrocrania norfolki Laurin, 1992, Tonga, BORDAU 2, stn DW 1602, 263-320 m, outer, inner and tilted views of dorsal valve, MNHN IB-2013-679. D-H - Basiliola lucida (Gould, 1862); (D-E) inner and oblique views of posterior part of dorsal valve, MNHN IB-2013-700, SEM, stn DW 1635, 320-323 m; (F-H) dorsal, lateral and anterior views of articulated specimen, MNHN IB-2013-699, stn DW 1587, 309-400 m. I-M - Basiliola beecheri (Dall, 1895), BORDAU 2; (I-K) dorsal, lateral and anterior views of articulated specimen, MHNH IB-2013-694, stn DW 1619, 591-593 m; (L-M) inner and oblique views of posterior part of dorsal valve, MNHN IB-2013- 683, SEM, stn CP 1545, 444-447 m. N-S - Basiliolella colurnus (Hedley, 1905), BORDAU 2; (N-Q) dorsal, lateral views and dorsal, anterior views of two articulated specimens, MNHN IB-2013-706, stn CP 1545, 444-447 m; (R-S) inner and oblique views of posterior part of dorsal valve, MNHN IB-2013-703, SEM, stn DW 1536, 320-323 m. 590 Bitner M.A. Order Rhynchonellida Kuhn, 1949 1895 Hemithyris beecheri Dall, p. 717, pl. 31, figs. 1-4. 2008 Basiliola beecheri - Bitner, pp. 427-428, fig. 5H-L cum( syn.). Superfamily Pugnacoidea Rzhonsnitskaya, 1956 2009 Basiliola beecheri - Bitner, p. 6-7, fig. 3D, E. Family Basiliolidae Cooper, 1959 2010 Basiliola beecheri - Zezina, p. 1179. Genus Basiliola Dall, 1908 2015 Basiliola beecheri - Bitner, pp. 35-36, fig. 2G-H. Type species - Hemithyris beecheri Dall, 1895, by original designation of Material examined: Tonga, BORDAU 2 cruise, stn DW Dall (1908: 442) 1509, one articulated specimen (MNHN IB-2009-544); stn CP 1510, 7 articulated specimens (MNHN IB-2013-681); stn DW Basiliola lucida (Gould, 1862) 1538, 2 articulated specimens (MNHN IB-2009-545); stn CP 1539, 2 articulated specimens (MNHN IB-2009-542); stn DW 1543, one Fig. 2D-H articulated specimen (MNHN IB-2013-682); stn DW 1544, one articulated specimen (MNHN IB-2009-540); stn CP 1545, 15 arti- 1862 Rhynchonella lucida Gould, p. 120. culated specimens, one ventral and one dorsal valves (MNHN IB- 2008 Basiliola lucida - Bitner, p. 427, fig. 5A-G cum( syn.). 2009-538, IB-2013-683); stn CP 1546, 2 articulated specimens and 2009 Basiliola lucida - Bitner, p. 7, fig. 3A-C. one dorsal valve (MNHN IB-2009-541); stn DW 1548, one articu- 2010 Basiliola lucida - Zezina, p. 1179. lated specimen (MNHN IB-2013-684); stn DW 1554, one articula- 2015 Basiliola lucida - Bitner, p. 36, fig. 2C-D. ted specimen (MNHN IB-2013-685); stn DW 1555, one articulated specimen (MNHN IB-2013-686); stn CH 1557, one articulated spe- Material examined: Tonga, BORDAU 2 cruise, stn DW 1516, 4 articulated specimens
Recommended publications
  • Brachiopoda from the Southern Indian Ocean (Recent)
    I - MMMP^j SA* J* Brachiopoda from the Southern Indian Ocean (Recent) G. ARTHUR COOPER m CONTRIBUTIONS TO PALEOBIOLOGY • NUMBER SERIES PUBLICATIONS OF THE SMITHSONIAN INSTITUTION Emphasis upon publication as a means of "diffusing knowledge" was expressed by the first Secretary of the Smithsonian. In his formal plan for the Institution, Joseph Henry outlined a program that included the following statement: "It is proposed to publish a series of reports, giving an account of the new discoveries in science, and of the changes made from year to year in all branches of knowledge." This theme of basic research has been adhered to through the years by thousands of titles issued in series publications under the Smithsonian imprint, commencing with Smithsonian Contributions to Knowledge in 1848 and continuing with the following active series: Smithsonian Contributions to Anthropology Smithsonian Contributions to Astrophysics Smithsonian Contributions to Botany Smithsonian Contributions to the Earth Sciences Smithsonian Contributions to the Marine Sciences Smithsonian Contributions to Paleobiology Smithsonian Contributions to Zoology Smithsonian Studies in Air and Space Smithsonian Studies in History and Technology In these series, the Institution publishes small papers and full-scale monographs that report the research and collections of its various museums and bureaux or of professional colleagues in the world of science and scholarship. The publications are distributed by mailing lists to libraries, universities, and similar institutions throughout the world. Papers or monographs submitted for series publication are received by the Smithsonian Institution Press, subject to its own review for format and style, only through departments of the various Smithsonian museums or bureaux, where the manuscripts are given substantive review.
    [Show full text]
  • The Present-Day Mediterranean Brachiopod Fauna: Diversity, Life Habits, Biogeography and Paleobiogeography*
    SCI. MAR., 68 (Suppl. 1): 163-170 SCIENTIA MARINA 2004 BIOLOGICAL OCEANOGRAPHY AT THE TURN OF THE MILLENIUM. J.D. ROS, T.T. PACKARD, J.M. GILI, J.L. PRETUS and D. BLASCO (eds.) The present-day Mediterranean brachiopod fauna: diversity, life habits, biogeography and paleobiogeography* A. LOGAN1, C.N. BIANCHI2, C. MORRI2 and H. ZIBROWIUS3 1 Centre for Coastal Studies and Aquaculture, University of New Brunswick, Saint John, N.B. E2L 4L5, Canada. E-mail: [email protected] 2 DipTeRis (Dipartimento Territorio e Risorse), Università di Genova, Corso Europa 26, I-16132 Genoa, Italy. 3 Centre d’Océanologie de Marseille, Station Marine d’Endoume, Rue Batterie des Lions, 13007 Marseilles, France. SUMMARY: The present-day brachiopods from the Mediterranean Sea were thoroughly described by nineteenth-century workers, to the extent that Logan’s revision in 1979 listed the same 11 species as Davidson, almost 100 years earlier. Since then recent discoveries, mainly from cave habitats inaccessible to early workers, have increased the number of species to 14. The validity of additional forms, which are either contentious or based on scanty evidence, is evaluated here. Preferred substrates and approximate bio-depth zones of all species are given and their usefulness for paleoecological reconstruction is discussed. A previous dearth of material from the eastern Mediterranean has now been at least partially remedied by new records from the coasts of Cyprus, Israel, Egypt, and, in particular, Lebanon and the southern Aegean Sea. While 11 species (79 % of the whole fauna) have now been recorded from the eastern basin, Terebratulina retusa, Argyrotheca cistellula, Megathiris detruncata and Platidia spp.
    [Show full text]
  • Mise En Page 1
    BITNER M. A., 2007. Shallow water brachiopod species of New Caledonia, in: Payri C.E., Richer de Forges B. (Eds.) Compendium of marine species of New Caledonia, Doc. Sci. Tech. II7, seconde édition, IRD Nouméa, p. 171 Shallow water brachiopod species of New Caledonia Maria Aleksandra BITNER Institute of Paleobiology, Polish Academy of Sciences, ul. Tawarda 51/55, 00-818 Warszawa Poland [email protected] Brachiopods are entirely marine, sessile, benthic invertebrates with soft body enclosed in a shell con - sisting of two valves which differ in size, shape, and sometimes even in ornamentation and colour. Most brachiopods have calcareous shell, except lingulids which have organophosphatic shell. They have a very long and impressive geological history but today they are regarded as a minor phylum and are reduced to about 110 genera. Nevertheless, brachiopods are widely distributed, being present in all of the world’s oceans and they can locally dominate the benthic marine communities. Their bathymetric range is very wide, from the intertidal zone to depths of about 6000 meters, however, most commonly they occur from 100 to 500 m. Among the 30 brachiopod species occurring in the New Caledonia region (d’Hondt 1987; Emig 1988; Laurin 1997), only four of them have been found in the shallow water less than 100 meters deep. The shallow water brachiopod fauna consists of 4 species belonging to 3 genera, in 3 families, 3 orders (Lingulida, Terebratulida and Thecideida) and 2 subphyla (Linguliformea and Rhynchonelliformea). Two Lingula species, namely L. anatina Lamarck and L. adamsi Dall, are recognised in New Caledonia.
    [Show full text]
  • A Note on Dallina Septigera (Loven), (Brachiopoda, Dallinidae)
    J. mar. bioi. Ass. U.K. (1960) 39, 91-99 91 Printed in Great Britain A NOTE ON DALLINA SEPTIGERA (LOVEN), (BRACHIOPODA, DALLINIDAE) By D. ATKINS,D.Sc. From the Plymouth Laboratory (Plate I and Text-figs. 1-5) The discovery of a homoeomorph, Pallax dalliniformis, of Dallina septigera (Loven) dredged with that species (Atkins, 1960) and, it is believed, some• times confused with it, certainly by Fischer & Oehlert (1891), has made a brief redescription desirable. During the present work more than a hundred D. septigera of shell length 5-31 mm have been obtained, and most of them examined internally. The original description in Latin-without figures-of Dallina septigera (= Terebratula septigera) was by Loven in 1846 (p. 183). Unfortunately his description does not now clearly separate his species from Pallax dallini• formis, except perhaps his failure to mention the presence of dental plates, pedicle collar and spiculation. It is doubtful how much weight can be attached to this, for on the same page he failed to mention the presence of dental plates in Macandrevia cranium. He gave the length as 28 mm, width as 21·5 mm and depth as 17 mm. The Stockholm Natural History Museum, the most likely Museum to possess Loven's type specimen, unfortunately does not have it, and it is probable that he did not designate one. The Museum, however, does possess old collections of dried shells of this species from Norway and the ~orth Sea, which Loven probably studied. Through the kindness of Dr H.Mutvei a large specimen from these was loaned to me: he stated that it is not known with certainty whether it was collected before or after 1846-the date of publication of Loven's paper.
    [Show full text]
  • Shell Microstructures in Lopingian Brachiopods: Implications for Fabric Evolution and Calcification
    Rivista Italiana di Paleontologia e Stratigrafia (Research in Paleontology and Stratigraphy) vol. 123(3): 541-560. November 2017 SHELL MICROSTRUCTURES IN LOPINGIAN BRACHIOPODS: IMPLICATIONS FOR FABRIC EVOLUTION AND CALCIFICATION CLAUDIO GARBELLI State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, 39 East Beijing Road, Nanjing, Jiangsu 210008, P.R. China. Dipartimento di Scienze della Terra A. Desio, Università di Milano, Via Mangiagalli 34, 20133 Milan, Italy. E-mail: [email protected] To cite this article: Garbelli C. (2017) - Shell microstructures in Lopingian brachiopods: implications for fabric evolution and calcification. Riv. It. Paleontol. Strat., 123(3): 541-560. Keywords: Rhynchonelliformea; Strophomenata; biomineralization; taxonomy; columnar layer. Abstract. The study of the shell microstructure of brachiopods is fundamental to understand their evolu- tionary history and their biomineralization process. Here, species of forty Lopingian brachiopods genera, represen- tative of twenty-seven different families, are investigated using the Scanning Electron Microscope. The investiga- ted specimens come from different paleogeographic localities in the Palaeotethys/Neotethys oceans. The studied brachiopods show a large variability of the shell fabric, which is mainly related to the organization of its structural units: laminae, fibers and columns, possibly crossed by pseudopunctae or punctae. For the Strophomenata, the laminar fabric of Productida is crossed by pseudopunctae with taleolae and the laminae are often organized in packages, with the blades oriented about perpendicular to each other; this feature is less evident in the laminar Or- thotetida, which bear pseudopunctae without taleoae. For the Rhynchonellata, fibrous fabrics are either impuctate in the Spiriferida, most Athyridida and Rhynchonellida, or with punctae, as observed in the Orthida, Terebratulida and in the Neoretziidae (Athyridida).
    [Show full text]
  • Dimerelloid Rhynchonellide Brachiopods in the Lower Jurassic of the Engadine (Canton Graubünden, National Park, Switzerland)
    1661-8726/08/010203–20 Swiss J. Geosci. 101 (2008) 203–222 DOI 10.1007/s00015-008-1250-8 Birkhäuser Verlag, Basel, 2008 Dimerelloid rhynchonellide brachiopods in the Lower Jurassic of the Engadine (Canton Graubünden, National Park, Switzerland) HEINZ SULSER & HEINZ FURRER * Key words: brachiopoda, Sulcirostra, Carapezzia, new species, Lower Jurassic, Austroalpine ABSTRACT ZUSAMMENFASSUNG New brachiopods (Dimerelloidea, Rhynchonellida) from Lower Jurassic Neue Brachiopoden (Dimerelloidea, Rhynchonellida) aus unterjurassischen (?lower Hettangian) hemipelagic sediments of the Swiss National Park in hemipelagischen Sedimenten (?unteres Hettangian) des Schweizerischen Na- south-eastern Engadine are described: Sulcirostra doesseggeri sp. nov. and tionalparks im südöstlichen Engadin werden als Sulcirostra doesseggeri sp. Carapezzia engadinensis sp. nov. Sulcirostra doesseggeri is externally similar to nov. und Carapezzia engadinensis sp. nov. beschrieben. Sulcirostra doesseggeri S. fuggeri (FRAUSCHER 1883), a dubious species, that could not be included in ist äusserlich S. fuggeri (FRAUSCHER 1883) ähnlich, einer zweifelhaften Spezies, a comparative study, because relevant samples no longer exist. A single speci- die nicht in eine vergleichende Untersuchung einbezogen werden konnte, weil men was tentatively assigned to Sulcirostra ?zitteli (BÖSE 1894) by comparison kein relevantes Material mehr vorhanden ist. Ein einzelnes Exemplar wird als of its external morphology with S. zitteli from the type locality. The partly Sulcirostra ?zitteli (BÖSE 1894) bezeichnet, im Vergleich mit der Aussenmor- silicified brachiopods are associated with sponge spicules, radiolarians and phologie von S. zitteli der Typuslokalität. Die teilweise silizifizierten Brachio- crinoid ossicles. Macrofossils are rare: dictyid sponges, gastropods, bivalves, poden waren mit Schwammnadeln, Radiolarien und Crinoiden-Stielgliedern crustaceans, shark teeth and scales of an actinopterygian fish. The Lower Ju- assoziiert.
    [Show full text]
  • Tertiary and Quaternary Brachiopods from the Southwest Pacific
    Tertiary and Quaternary Brachiopods from the Southwest Pacific G. ARTHUR COOPER SMITHSONIAN CONTRIBUTIONS TO PALEOBIOLOGY NUMBER 38 SERIES PUBLICATIONS OF THE SMITHSONIAN INSTITUTION Emphasis upon publication as a means of "diffusing knowledge" was expressed by the first Secretary of the Smithsonian. In his formal plan for the Institution, Joseph Henry outlined a program that included the following statement: "It is proposed to publish a series of reports, giving an account of the new discoveries in science, and of the changes made from year to year in all branches of knowledge." This theme of basic research has been adhered to through the years by thousands of titles issued in series publications under the Smithsonian imprint, commencing with Smithsonian Contributions to Knowledge in 1848 and continuing with the following active series: Smithsonian Contributions to Anthropology Smithsonian Contributions to Astrophysics Smithsonian Contributions to Botany Smithsonian Contributions to the Earth Sciences Smithsonian Contributions to the Marine Sciences Smithsonian Contributions to Paleobiology Smithsonian Contributions to Zoology Smithsonian Studies in Air and Space Smithsonian Studies in History and Technology In these series, the Institution publishes small papers and full-scale monographs that report the research and collections of its various museums and bureaux or of professional colleagues in the world of science and scholarship. The publications are distributed by mailing lists to libraries, universities, and similar institutions throughout the world. Papers or monographs submitted for series publication are received by the Smithsonian Institution Press, subject to its own review for format and style, only through departments of the various Smithsonian museums or bureaux, where the manuscripts are given substantive review.
    [Show full text]
  • Download Full Article in PDF Format
    Récent Brachiopoda from the océanographie expédition SEAMOUNT 2 to the north-eastern Atlantic in 1993 Alan LOGAN Centre for Coastal Studies and Aquaculture, University of New Brunswick, P.O. Box 5050, Saint John, N.B., E2L4L5 (Canada) [email protected] Logan A. 1998. — Recent Brachiopoda from the oceanographic expedition SEAMOUNT 2 to the north-eastern Atlantic in 1993. Zoosystema 20 (4) : 549-562. ABSTRACT Eight species of recent brachiopods belonging to the genera Neocrania, Dyscolia, Abyssothyris, Stenosarina, Eucalathis, Platidia, Phaneropora and Dallinahsve been identified from collections from the 1993 SEAMOUNT 2 expedition to Meteor, Hyeres, Irving-Cruiser, Plato, Atlantis, Tyro and Antialtair seamounts in the north-eastern Atlantic. The species misidentified by Jeffreys (1878) as Terebratula vitrea var. sphenoidea [non Philippi, 1844] is described as Stenosarina davidsoni n.sp. The affinities of the SEAMOUNT 2 brachiopods are with the Mauritanian biogeographic province. Diversity and number of stations yielding brachiopods increase from south to north in the cluster of six seamounts (Meteor-Tyro) south of the Azores. Brachiopod diversity for the seven seamounts as a whole is less than for the Canary Islands to the east. There is an as yet unexplained absence from the sea- KEY WORDS mounts of deeper water species belonging to such genera as Pelagodiscus, Brachk>pods, Hispanirhynchia, Terebratulina, Gryphus, Megerlia and Macandrevia, which SEAMOUNT 2 commonly occur around island archipelagos such as Madeira, the Canaries and north-eastern Atlantic. the Cape Verdes, as well as off the Iberian coast and the African mainland. • 1998 • 20(4) 549 Logan A. RÉSUMÉ Brachiopodes actuels récoltés lors de l'expédition océanographique SEA­ MOUNT 2 dans l'océan Atlantique Nord-Est en 1993.
    [Show full text]
  • Did the Amalgamation of Continents Drive the End Ordovician Mass Extinctions?
    Palaeogeography, Palaeoclimatology, Palaeoecology 311 (2011) 48–62 Contents lists available at SciVerse ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo Did the amalgamation of continents drive the end Ordovician mass extinctions? Christian M.Ø. Rasmussen a,b,⁎, David A.T. Harper b,c,1 a Center for Macroecology, Evolution and Climate, Natural History Museum of Denmark, University of Copenhagen, Øster Voldgade 5–7, DK-1350 Copenhagen K, Denmark b Nordic Center for Earth Evolution (NordCEE), Natural History Museum of Denmark, University of Copenhagen, Øster Voldgade 5–7, DK-1350 Copenhagen K, Denmark c Geological Museum, Natural History Museum of Denmark, University of Copenhagen, Øster Voldgade 5–7, DK-1350 Copenhagen K, Denmark article info abstract Article history: Global biodiversity has been punctuated throughout the Phanerozoic by extinction events that vary in their Received 27 January 2011 degree of intensity and devastation. The mass extinction event that occurred at the end of the Ordovician Received in revised form 11 July 2011 Period rapidly removed a wide range of species. Because taxonomic loss occurred during an ice age, this is Accepted 28 July 2011 believed to have initiated the extinctions and thus, these extinctions have often been viewed as a deep time Available online 5 August 2011 analogue to the loss in species diversity during the present day glacial interval. The current study, however, indicates that temperature – though arguably being a trigger – was not the sole reason for the crisis. Based on Keywords: fi Ordovician a large, bibliographic database of rhynchonelliform brachiopods that speci cally operates within very narrow Silurian time-slices where every locality has been precisely georeferenced for the Upper Ordovician–Lower Silurian Brachiopods interval, we show that the extinctions were not uniformly distributed, nor was the succeeding recovery.
    [Show full text]
  • The Li Isotope Composition of Marine Biogenic Carbonates: Patterns and Mechanisms Mathieu Dellinger, A
    The Li isotope composition of marine biogenic carbonates: Patterns and Mechanisms Mathieu Dellinger, A. Joshua West, Guillaume Paris, Jess Adkins, Philip Pogge von Strandmann, Clemens Ullmann, Robert Eagle, Pedro Freitas, Marie-Laure Bagard, Justin Ries, et al. To cite this version: Mathieu Dellinger, A. Joshua West, Guillaume Paris, Jess Adkins, Philip Pogge von Strandmann, et al.. The Li isotope composition of marine biogenic carbonates: Patterns and Mechanisms. Geochimica et Cosmochimica Acta, Elsevier, 2018, 236, pp.315-335. 10.1016/j.gca.2018.03.014. insu-01741161 HAL Id: insu-01741161 https://hal-insu.archives-ouvertes.fr/insu-01741161 Submitted on 22 Mar 2018 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Accepted Manuscript The Li isotope composition of marine biogenic carbonates: Patterns and Mech- anisms Mathieu Dellinger, A. Joshua West, Guillaume Paris, Jess F. Adkins, Philip Pogge von Strandmann, Clemens V. Ullmann, Robert A. Eagle, Pedro Freitas, Marie-Laure Bagard, Justin B. Ries, Frank A. Corsetti, Alberto Perez-Huerta, Anthony R.
    [Show full text]
  • New Barremian Rhynchonellide Brachiopod from Serbia and The
    New Barremian rhynchonellide brachiopod genus from Serbia and the shell microstructure of Tetrarhynchiidae BARBARA RADULOVIĆ, NEDA MOTCHUROVA−DEKOVA, and VLADAN RADULOVIĆ Radulović, B., Motchurova−Dekova, N., and Radulović, V. 2007. New Barremian rhynchonellide brachiopod from Ser− bia and the shell microstructure of Tetrarhynchiidae. Acta Palaeontologica Polonica 52 (4): 761–782. A new rhynchonellide brachiopod genus Antulanella is erected based on the examination of the external and internal morphologies and shell microstructure of “Rhynchonella pancici”, a common species in the Barremian shallow−water limestones of the Carpatho−Balkanides of eastern Serbia. The new genus is assigned to the subfamily Viarhynchiinae, family Tetrarhynchiidae. The shell of Antulanella is small to rarely medium−sized, subglobose, subcircular, fully costate, with hypothyrid rimmed foramen. The dorsal euseptoidum is much reduced. The dental plates are thin, ventrally diver− gent. The hinge plates are straight to ventrally convex. The crura possess widened distal ends, rarely raduliform or canaliform. The shell is composed of two calcitic layers. The secondary layer is fine fibrous, homogeneous built up of predominantly anisometric anvil−like fibres. Although data on the shell microstructure of post−Palaeozoic rhyncho− nellides are still incomplete, it is possible to distinguish two types of secondary layer: (i) fine fibrous typical of the superfamilies Rhynchonelloidea and Hemithiridoidea and (ii) coarse fibrous typical of the superfamilies Pugnacoidea, Wellerelloidea, and Norelloidea. The new genus Antulanella has a fine fibrous microstructure of the secondary layer, which is consistent with its allocation in the Hemithiridoidea. Antulanella pancici occurs in association with other brachi− opods showing strong Peritethyan affinity and close resemblance to the Jura fauna (= Subtethyan fauna).
    [Show full text]
  • Permophiles International Commission on Stratigraphy
    Permophiles International Commission on Stratigraphy Newsletter of the Subcommission on Permian Stratigraphy Number 66 Supplement 1 ISSN 1684 – 5927 August 2018 Permophiles Issue #66 Supplement 1 8th INTERNATIONAL BRACHIOPOD CONGRESS Brachiopods in a changing planet: from the past to the future Milano 11-14 September 2018 GENERAL CHAIRS Lucia Angiolini, Università di Milano, Italy Renato Posenato, Università di Ferrara, Italy ORGANIZING COMMITTEE Chair: Gaia Crippa, Università di Milano, Italy Valentina Brandolese, Università di Ferrara, Italy Claudio Garbelli, Nanjing Institute of Geology and Palaeontology, China Daniela Henkel, GEOMAR Helmholtz Centre for Ocean Research Kiel, Germany Marco Romanin, Polish Academy of Science, Warsaw, Poland Facheng Ye, Università di Milano, Italy SCIENTIFIC COMMITTEE Fernando Álvarez Martínez, Universidad de Oviedo, Spain Lucia Angiolini, Università di Milano, Italy Uwe Brand, Brock University, Canada Sandra J. Carlson, University of California, Davis, United States Maggie Cusack, University of Stirling, United Kingdom Anton Eisenhauer, GEOMAR Helmholtz Centre for Ocean Research Kiel, Germany David A.T. Harper, Durham University, United Kingdom Lars Holmer, Uppsala University, Sweden Fernando Garcia Joral, Complutense University of Madrid, Spain Carsten Lüter, Museum für Naturkunde, Berlin, Germany Alberto Pérez-Huerta, University of Alabama, United States Renato Posenato, Università di Ferrara, Italy Shuzhong Shen, Nanjing Institute of Geology and Palaeontology, China 1 Permophiles Issue #66 Supplement
    [Show full text]